Ion Microprobe Measurements of Oxygen Isotope Compositions of Artificial Chondrule and CAI: Implication for Nebular Oxygen Exchange During the Formation of Chondrules and CAIs

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Scientific paper

SIMS measurements for O-isotopes of artificial chondrule and CAI show
that, if O2 partial pressure was high enough possibly by dissociation of
H2O, the mixing line observed in chondrites could be formed during the
formation of chondrules and CAIs.

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